| Introduction | Physical Setting | Methods | Results | Conclusions | Future Study | Proximity Map |
| Aerial Photo | Digital Elevation Map | Photo Essay | Chippewa Watershed | Who We Are | Acknowledgements | References |
Geologic History
Bedrock Geology Map
State Soils Map
Unconsolidated Materials Map
Glacial Map
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The climate at the Hubbard Site is temperate continental (Dfb according to the Koppen classification system). Climate date for Pepin county is supplied in the tables below. Links to Climate Data:
Average Temperature is the monthly mean of the daily (24 hour) temperature. Average Maximum Temperature is the monthly mean of the maximum daily temperature. Average Minimum Temperature is the monthly mean of the minimum daily temperature. In winter, the average temperature is 17.7 degrees Fahrenheit (F) and the average daily minimum temperature is 6.7 degrees. The lowest temperature on record, which occurred at Menomonie on February 3, 1996, was -40 degrees. In summer, the average temperature is 68.7 degrees and the average daily maximum temperature is 80.0 degrees. The highest temperature, which occurred at Menomonie on August 2, 1964, was 101 degrees. Averages
Daily Extremes
Back to Climate
PrecipitationAverage Rainfall is the mean monthly precipitation, including rain, snow, hail, etc.
Averages
Back to Climate
Snowfall
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| Jan | Feb | March | April | May | June | July | Aug | Sept | Oct | Nov | Dec | |
| Mean | 12.5" | 6.8" | 7.8" | 1.0" | 0.0" | 0.0" | 0.0" | 0.0" | 0.0" | 0.1" | 4.4" | 8.6" |
| High-Year | 33.3" / 1967 |
19.4" / 1962 |
25.4" / 1965 |
9.8" / 1965 |
0.0" | 0.0" | 0.0" | 0.0" | 0.0" | 4.8" / 1959 |
20.1" / 1991 |
11.7" // 1968 |
| Jan | Feb | March | April | May | June | July | August | Sept | Oct | Nov | Dec | |
| >.01" | 7.9 | 5.6 | 8.2 | 9.5 | 10.8 | 11.6 | 10.7 | 10.2 | 10.1 | 9.0 | 7.9 | 7.5 |
| >.5" | 0.1 | 0.2 | 0.8 | 1.5 | 2.4 | 3.3 | 2.6 | 2.5 | 2.7 | 1.1 | 1.2 | 0.3 |
| >1" | 0.0 | 0.0 | 0.3 | 0.5 | 0.7 | 1.3 | 1.1 | 1.2 | 0.9 | 0.3 | 0.3 | 0.1 |
| Base Temp-F | Median | Early | 90% | 10% | Late |
| 32° | 5 / 12 | 4 / 21 | 4 / 28 | 5 / 27 | 6 / 01 |
| 30° | 5 / 05 | 4 / 09 | 4 / 24 | 5 / 17 | 6 / 01 |
| 28° | 4 / 27 | 3 / 29 | 4 / 09 | 5 / 08 | 5 / 14 |
| 24° | 4 / 14 | 3 / 24 | 4 / 03 | 4 / 25 | 5 / 06 |
| 20° | 4 / 09 | 3 / 21 | 3 / 23 | 4 / 16 | 4 / 22 |
| 16° | 3 / 26 | 2 / 26 | 3 / 11 | 4 / 07 | 4 / 09 |
Date of First Fall Occurrence
(month / day)
| Base Temp-F | Median | Early | 90% | 10% | Late |
| 32 | 9 / 30 | 9 / 03 | 9 / 20 | 10 / 08 | 10 / 15 |
| 30 | 10 / 04 | 9 / 11 | 9 / 23 | 10 / 15 | 10 / 30 |
| 28 | 10 / 05 | 9 / 19 | 9 / 28 | 10 / 24 | 11 / 04 |
| 24 | 10 / 23 | 10 / 02 | 10 / 04 | 11 / 05 | 11 / 11 |
| 20 | 11 / 03 | 10 / 02 | 10 / 19 | 11 / 12 | 11 / 16 |
| 16 | 11 / 12 | 10 / 20 | 10 / 30 | 11 / 29 | 12 / 19 |
Growing Season: Based on the average length of growing season using three index temperatures at 10, 20, 50, 80, and 90% probabilities.
Daily Minimum Temperature
During Growing Season
| Probability | >24° | >28° | >32° |
| 9 Years in 10 | 165 | 147 | 119 |
| 8 Years in 10 | 172 | 153 | 125 |
| 5 Years in 10 | 187 | 165 | 138 |
| 2 Years in 10 | 202 | 177 | 150 |
| 1 Years in 10 | 210 | 180 | 157 |
Information regarding weather data was recorded for the period 1961-00 at : MENOMONIE SEWAGE PLANT, WI
Contributed by Group 3: Chris Drabandt, Lori Hafeman, LeRoy Molitor, and Melissa Peterson
Links to Vegetation Information:
Rare, Threatened,
and Endangered Species
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1Wisconsin
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Wisconsin Natural Heritage Inventory Map for Pepin County |
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The vegetation of Pepin County in 1965 was Southern oak forest (white, black, and red oaks), oak savanna (bur oak, white oak and bluestem), southern mesic forest (sugar maple, basswood, elm), prairie (bluestem and composites), lowland hard woods (willows, soft maple and ash).
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Back to Vegetation
Vegetation Pictures of the Hubbard Site
Contributed by Group 2: Erin Heidtke, Julie Sowka, and Rebecca Thorn
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The bedrock formations of Wisconsin were derived at the beginning of the Cambrian Period in the Paleozoic Era, as large shallow seas covered the present day Wisconsin landscape. These seas were the place of accumulation for vast amounts of sand, mud (high in lime), clays, and silts. These sediments were cemented and compressed by physical forces into sandstone, shale, limestone, and dolomite. Granite is predominately the bottom layer in this geologic time scale, and can be dated back as old as the earth itself (approximately 4.6 billion years). Above this lie the Mt. Simon, Eau Claire, and Wonewoc sandstone formations. There were possibly more types of sedimentary rock above these formations, but they have eroded away. The Ice age is presumed a major reason for the erosion of this area down to the sandstone formations. With the three major advances by glaciers covering most of the state from roughly 200,000 years ago until 10,000 years ago, the landscape changed dramatically and stirred up the ground into a huge hodgepodge of sediment that was carried many kilometers to its present location. These glaciers released large volumes of melt water in retreat, carved deep wide river valleys, and left extensive sand and gravel deposits. The soil building process was reset when the last glacier receded from this area, approximately 10,000 years ago. These soils have some interesting qualities that make them some of the more fertile soils on this continent as well as the entire world. These younger soils exhibit qualities that allow plants to get many of their nutrients form the ground, whereas older soils have had the vital nutrients leached out and therefore plants have to derive their nutrients from elsewhere.
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Links to Maps: |
Contributed by Group 8: Isaac Grace, Mike Selb, and Sandy Yassin